Labandeira Conrad C
Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, P.O. Box 37012, Washington, DC 20013-7012, USA.
Naturwissenschaften. 2013 Apr;100(4):355-64. doi: 10.1007/s00114-013-1035-4. Epub 2013 Mar 24.
A survey of the fossil record of land-plant tissues and their damage by arthropods reveals several results that shed light on trophic trends in host-plant resource use by arthropods. All 14 major plant tissues were present by the end of the Devonian, representing the earliest 20% of the terrestrial biota. During this interval, two types of time lags separate the point between when tissues first originated from their earliest consumption by herbivorous arthropods. For epidermis, parenchyma, collenchyma and xylem, live tissue consumption was rapid, occurring on average 10 m.y. after the earliest tissue records. By contrast, structural tissues (periderm, sclerenchyma), tissues with actively dividing cells (apical, lateral, intercalary meristems), and reproductive tissues (spores, megagametophytes, integuments) experienced approximately a 9-fold (92 m.y.) delay in arthropod herbivory, extending well into the Carboniferous Period. Phloem similarly presents a delay of 85 m.y., but this incongruously long lag-time may be attributed to the lack of preservation of this tissue in early vascular plants. Nevertheless, the presence of phloem can be indicated from planar spaces adjacent well-preserved xylem, or inferred from a known anatomy of the same plant taxon in better preserved material, especially permineralisations. The trophic partitioning of epidermis, parenchyma, phloem and xylem increases considerably to the present, probably a consequence of dietary specialization or consumption of whole leaves by several herbivore functional feeding groups. Structural tissues, meristematic tissues and reproductive tissues minimally have been consumed throughout the fossil record, consistent with their long lags to herbivory during the earlier Paleozoic. Neither angiosperm dominance in floras nor global environmental perturbations had any discernible effect on herbivore trophic partitioning of plant tissues.
一项关于陆地植物组织化石记录及其受节肢动物损害情况的调查揭示了几个结果,这些结果有助于阐明节肢动物在宿主植物资源利用方面的营养趋势。到泥盆纪末期,所有14种主要植物组织都已出现,这代表了陆地生物群最早的20%。在此期间,两种时间滞后将组织首次起源的时间点与草食性节肢动物最早消耗它们的时间点分隔开来。对于表皮、薄壁组织、厚角组织和木质部,活组织的消耗很快,最早的组织记录出现后平均1000万年就发生了。相比之下,结构组织(周皮、厚壁组织)、具有活跃分裂细胞的组织(顶端分生组织、侧生分生组织、居间分生组织)和生殖组织(孢子、大配子体、珠被)在节肢动物取食方面经历了大约9倍(9200万年)的延迟,一直持续到石炭纪。韧皮部同样有8500万年的延迟,但这种异常长的滞后时间可能归因于早期维管植物中这种组织保存不佳。尽管如此,韧皮部的存在可以从保存完好的木质部相邻的平面空间中推断出来,或者从保存更好的材料(尤其是矿化化石)中同一植物分类群的已知解剖结构中推断出来。表皮、薄壁组织、韧皮部和木质部的营养分配到现在有了显著增加,这可能是饮食专业化或几个草食动物功能取食组消耗整叶的结果。在整个化石记录中,结构组织、分生组织和生殖组织极少被消耗,这与它们在古生代早期取食滞后时间长是一致的。植物群中被子植物的优势地位和全球环境扰动对节肢动物在植物组织上的营养分配都没有明显影响。